Understanding Hazardous Earth for Edexcel B Geography - GCSE and A Level Notes

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Nima K

01/07/2022

Geography

Hazardous Earth

Subjects

Geography

Understanding Hazardous Earth for Edexcel B Geography - GCSE and A Level Notes

Name: Knowunity
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Understanding Tectonic Hazards and Earth's Systems - A comprehensive guide covering Earth's structure, volcanic activity, earthquakes, and climate systems for GCSE Geography Edexcel B.

• Detailed exploration of Earth structure including core, mantle, and crust layers
• Analysis of plate boundaries and their interactions
• Coverage of volcanic formations and earthquake impacts
• Examination of global atmospheric circulation and climate change
• In-depth study of tropical cyclones and their formation

...

01/07/2022

939

Topic 1: Hazardous Earth: Tectonic Hazards
What you need to be able to do / understand
I can interpret a cross-section of the Earth to show

View

Volcanoes and Hotspots

Hazardous earth geography Edexcel B bbc bitesize covers various volcanic formations, including hotspots and different volcano types.

Hotspots are formed when:

Hot magma plumes rise from the mantle
They burn through weaker parts of the crust
Volcanoes and islands are created
The plume remains stationary while plates move, creating island chains

Example: The Hawaiian Islands are a prime example of a hotspot volcanic chain.

There are two main types of volcanoes:

Shield volcanoes:
- Runny, fast-flowing lava
- Low viscosity
- Non-explosive
- Shallow-sided (flat)
Composite volcanoes:
- Viscous, slow-flowing lava
- High-pressure magma
- Explosive
- Steep-sided

Highlight: Understanding the differences between these volcano types is crucial for GCSE Geography Hazardous Earth past papers.

View

Earthquakes and Tsunamis

Earthquakes occur when pressure builds up and is released as plates shift. The Richter scale measures earthquake strength logarithmically, with each number being 10 times stronger than the previous.

Earthquake characteristics vary:

Conservative and convergent boundaries: destructive, shallow earthquakes
Divergent boundaries: smaller earthquakes

Definition: A tsunami is a large wave caused by the displacement of water during an oceanic earthquake.

Tsunami formation process:

Oceanic crust jolts during an earthquake
Water above the plate is displaced
Water travels fast with low amplitude
As it approaches the coast, friction with the seabed causes waves to slow and gain height
A wall of water forms, typically 10 feet high but can reach 100 feet

Highlight: Understanding tsunami formation is essential for Understanding tectonic hazards in geography Edexcel B questions.

View

Earthquake Impacts and Management

GCSE Geography Edexcel B Hazardous Earth questions often focus on the impacts of earthquakes in developed and developing countries.

Japan Earthquake 2011 (Developed country):

Primary impacts: 15,900 deaths, 350,000 homeless, damaged infrastructure
Secondary impacts: Nuclear reactor meltdown, economic disruption

Haiti Earthquake 2010 (Developing country):

Primary impacts: 316,000 deaths, 1 million homeless, damaged infrastructure
Secondary impacts: Cholera outbreak, job losses, displacement

Example: The Japan earthquake caused $235 billion in damage, making it the costliest in history.

Earthquake management strategies include:

Short-term relief: Providing shelter and supplies
Long-term planning: Training and funding emergency services
Preparation: Implementing warning systems and evacuation plans

Highlight: Effective earthquake management is crucial for minimizing impacts and saving lives.

View

Plate Boundaries and Earth's Structure

Structure of the Earth a level Geography delves deeper into the Earth's layers and their properties. The Earth's structure plays a crucial role in tectonic activity and hazard formation.

Key components of the Earth's structure:

Inner core:
- Solid state
- Composed of iron and nickel
- Extremely high pressure
- Contains uranium and radioactive elements
- Temperature around 5000°C
- Source of Earth's internal energy
Outer core:
- Molten state
- Composed of iron and nickel
- Convection currents occur here
- Transfers heat to the mantle
Mantle:
- Solid at lower levels, liquid (dense fluid) at the top
- Contains the asthenosphere
- Convection currents here cause lithosphere movement
Lithosphere:
- Solid state
- Includes the crust and uppermost mantle
- Contains tectonic plates
- Divided into continental and oceanic crust

Vocabulary: Lithosphere a level Geography refers to the rigid outer layer of the Earth that includes the crust and uppermost mantle.

Understanding plate boundaries is essential for Understanding tectonic hazards in geography Edexcel B answers:

Divergent boundaries:
- Plates move apart
- Associated with sea floor spreading
- Volcanoes form as magma rises from the mantle
Convergent boundaries:
- Plates collide
- Can involve oceanic-continental or oceanic-oceanic plate interactions
- Often associated with subduction zones and deep ocean trenches
Conservative boundaries:
- Plates slide past each other
- Friction builds between plates, leading to earthquakes

Definition: Types of plate boundaries gcse include divergent (constructive), convergent (destructive), and conservative.

View

Volcanic Activity and Hotspots

Hazardous Earth edexcel B curriculum covers various aspects of volcanic activity, including hotspots and different types of volcanoes.

Hotspot formation:

Hot magma plumes rise from the mantle
These plumes burn through weaker parts of the crust
Volcanoes and islands form above the hotspot
As tectonic plates move, the stationary plume creates a chain of islands or volcanoes

Example: The Hawaiian Islands are a classic example of hotspot volcanism, with a chain of islands formed as the Pacific Plate moves over a stationary hotspot.

Volcano types and characteristics:

Shield volcanoes:
- Formed by runny, fast-flowing lava
- Low viscosity magma
- Non-explosive eruptions
- Shallow-sided (flat) profile
- Example: Mauna Loa in Hawaii
Composite volcanoes:
- Formed by viscous, slow-flowing lava
- High-pressure magma
- Explosive eruptions
- Steep-sided profile
- Often produce pyroclastic flows and ash clouds
- Example: Mount Fuji in Japan

Highlight: Understanding the differences between shield and composite volcanoes is crucial for answering Understanding tectonic hazards in geography Edexcel B questions.

View

Earthquakes and Tsunami Formation

GCSE Geography Hazardous Earth past papers often include questions about earthquake mechanics and tsunami formation.

Earthquake occurrence:

Pressure builds up along fault lines
When the pressure exceeds the friction holding the plates together, they suddenly shift
Energy is released in the form of seismic waves

Earthquake characteristics:

Magnitude: Measured on the Richter scale (logarithmic)
Depth: Shallow earthquakes (close to surface) are often more severe
Location: Varies based on plate boundary type

Vocabulary: The focus is the point within the Earth where an earthquake originates, while the epicenter is the point on the Earth's surface directly above the focus.

Tsunami formation process:

An earthquake occurs under the ocean, jolting the oceanic crust
The water above the plate is displaced
This displacement creates a series of waves that travel outward from the epicenter
In deep water, tsunamis travel fast but with low amplitude
As the waves approach shallower coastal areas, they slow down due to friction with the seabed
This slowing causes the waves to increase in height, forming a wall of water
Tsunami waves can reach heights of 10 to 100 feet when they make landfall

Highlight: Understanding tsunami formation is crucial for coastal communities in tectonically active regions to prepare for and mitigate potential impacts.

View

Earthquake Impacts and Management Strategies

Understanding tectonic hazards in geography Edexcel B free resources often compare earthquake impacts in developed and developing countries. Two significant case studies are the 2011 Japan earthquake and the 2010 Haiti earthquake.

Japan Earthquake 2011 (Developed country):

Magnitude: 9.0
Focus depth: 30km
Epicenter: 70km from coast in Sendai Bay

Primary impacts:

15,900 deaths (93% from drowning)
2,800 missing
6,150 injured
350,000 homeless

Secondary impacts:

Two nuclear reactors went into meltdown
Airports closed
Motorways damaged
Oil refinery set on fire
$235 billion in damage (costliest earthquake in history)

Haiti Earthquake 2010 (Developing country):

Magnitude: 7.0
Focus depth: 13km
Epicenter: 25km from Port-au-Prince (population 2.5 million)

Primary impacts:

316,000 deaths
300,000 injured
1 million homeless

Secondary impacts:

Cholera outbreak
1/5 of jobs lost
Factories and businesses destroyed
Port, communication, and roads damaged and blocked

Highlight: The stark difference in death tolls despite the lower magnitude of the Haiti earthquake highlights the importance of infrastructure and preparedness in mitigating earthquake impacts.

Earthquake management strategies:

Short-term relief:

Providing emergency shelter (e.g., tents, temporary housing)
Distributing food, water, and medical supplies
Search and rescue operations

Long-term planning:

Training and funding emergency services
Implementing building codes for earthquake-resistant structures
Developing and maintaining early warning systems

Preparation:

Public education on earthquake safety
Regular earthquake drills
Creating and updating evacuation plans

Example: Japan's extensive earthquake preparation, including strict building codes and public education, helped limit the death toll despite the earthquake's massive magnitude.

Understanding these impacts and management strategies is crucial for answering Understanding tectonic hazards in geography Edexcel B questions and preparing for future seismic events.

View

Page 8: Tropical Cyclone Formation

Details the process of tropical cyclone development.

Definition: The Coriolis effect causes tropical cyclones to spin clockwise in the Southern Hemisphere and counterclockwise in the Northern Hemisphere.

Highlight: Warm ocean temperatures of at least 26-27°C are required for tropical cyclone formation.

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Subjects

Geography

Understanding Hazardous Earth for Edexcel B Geography - GCSE and A Level Notes

Nima K

@nspidka480

345 Followers

Understanding Tectonic Hazards and Earth's Systems - A comprehensive guide covering Earth's structure, volcanic activity, earthquakes, and climate systems for GCSE Geography Edexcel B.

...

01/07/2022

939

11/10

Geography

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Volcanoes and Hotspots

Hazardous earth geography Edexcel B bbc bitesize covers various volcanic formations, including hotspots and different volcano types.

Hotspots are formed when:

Hot magma plumes rise from the mantle
They burn through weaker parts of the crust
Volcanoes and islands are created
The plume remains stationary while plates move, creating island chains

Example: The Hawaiian Islands are a prime example of a hotspot volcanic chain.

There are two main types of volcanoes:

Shield volcanoes:
- Runny, fast-flowing lava
- Low viscosity
- Non-explosive
- Shallow-sided (flat)
Composite volcanoes:
- Viscous, slow-flowing lava
- High-pressure magma
- Explosive
- Steep-sided

Highlight: Understanding the differences between these volcano types is crucial for GCSE Geography Hazardous Earth past papers.

Sign up to see the content. It's free!

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Join milions of students

By signing up you accept Terms of Service and Privacy Policy

Earthquakes and Tsunamis

Earthquakes occur when pressure builds up and is released as plates shift. The Richter scale measures earthquake strength logarithmically, with each number being 10 times stronger than the previous.

Earthquake characteristics vary:

Conservative and convergent boundaries: destructive, shallow earthquakes
Divergent boundaries: smaller earthquakes

Definition: A tsunami is a large wave caused by the displacement of water during an oceanic earthquake.

Tsunami formation process:

Oceanic crust jolts during an earthquake
Water above the plate is displaced
Water travels fast with low amplitude
As it approaches the coast, friction with the seabed causes waves to slow and gain height
A wall of water forms, typically 10 feet high but can reach 100 feet

Highlight: Understanding tsunami formation is essential for Understanding tectonic hazards in geography Edexcel B questions.

Sign up to see the content. It's free!

Access to all documents

Improve your grades

Join milions of students

By signing up you accept Terms of Service and Privacy Policy

Earthquake Impacts and Management

GCSE Geography Edexcel B Hazardous Earth questions often focus on the impacts of earthquakes in developed and developing countries.

Japan Earthquake 2011 (Developed country):

Primary impacts: 15,900 deaths, 350,000 homeless, damaged infrastructure
Secondary impacts: Nuclear reactor meltdown, economic disruption

Haiti Earthquake 2010 (Developing country):

Primary impacts: 316,000 deaths, 1 million homeless, damaged infrastructure
Secondary impacts: Cholera outbreak, job losses, displacement

Example: The Japan earthquake caused $235 billion in damage, making it the costliest in history.

Earthquake management strategies include:

Short-term relief: Providing shelter and supplies
Long-term planning: Training and funding emergency services
Preparation: Implementing warning systems and evacuation plans

Highlight: Effective earthquake management is crucial for minimizing impacts and saving lives.

Sign up to see the content. It's free!

Access to all documents

Improve your grades

Join milions of students

By signing up you accept Terms of Service and Privacy Policy

Plate Boundaries and Earth's Structure

Structure of the Earth a level Geography delves deeper into the Earth's layers and their properties. The Earth's structure plays a crucial role in tectonic activity and hazard formation.

Key components of the Earth's structure:

Inner core:
- Solid state
- Composed of iron and nickel
- Extremely high pressure
- Contains uranium and radioactive elements
- Temperature around 5000°C
- Source of Earth's internal energy
Outer core:
- Molten state
- Composed of iron and nickel
- Convection currents occur here
- Transfers heat to the mantle
Mantle:
- Solid at lower levels, liquid (dense fluid) at the top
- Contains the asthenosphere
- Convection currents here cause lithosphere movement
Lithosphere:
- Solid state
- Includes the crust and uppermost mantle
- Contains tectonic plates
- Divided into continental and oceanic crust

Vocabulary: Lithosphere a level Geography refers to the rigid outer layer of the Earth that includes the crust and uppermost mantle.

Understanding plate boundaries is essential for Understanding tectonic hazards in geography Edexcel B answers:

Divergent boundaries:
- Plates move apart
- Associated with sea floor spreading
- Volcanoes form as magma rises from the mantle
Convergent boundaries:
- Plates collide
- Can involve oceanic-continental or oceanic-oceanic plate interactions
- Often associated with subduction zones and deep ocean trenches
Conservative boundaries:
- Plates slide past each other
- Friction builds between plates, leading to earthquakes

Definition: Types of plate boundaries gcse include divergent (constructive), convergent (destructive), and conservative.

Sign up to see the content. It's free!

Access to all documents

Improve your grades

Join milions of students

By signing up you accept Terms of Service and Privacy Policy

Volcanic Activity and Hotspots

Hazardous Earth edexcel B curriculum covers various aspects of volcanic activity, including hotspots and different types of volcanoes.

Hotspot formation:

Hot magma plumes rise from the mantle
These plumes burn through weaker parts of the crust
Volcanoes and islands form above the hotspot
As tectonic plates move, the stationary plume creates a chain of islands or volcanoes

Example: The Hawaiian Islands are a classic example of hotspot volcanism, with a chain of islands formed as the Pacific Plate moves over a stationary hotspot.

Volcano types and characteristics:

Shield volcanoes:
- Formed by runny, fast-flowing lava
- Low viscosity magma
- Non-explosive eruptions
- Shallow-sided (flat) profile
- Example: Mauna Loa in Hawaii
Composite volcanoes:
- Formed by viscous, slow-flowing lava
- High-pressure magma
- Explosive eruptions
- Steep-sided profile
- Often produce pyroclastic flows and ash clouds
- Example: Mount Fuji in Japan

Highlight: Understanding the differences between shield and composite volcanoes is crucial for answering Understanding tectonic hazards in geography Edexcel B questions.

Sign up to see the content. It's free!

Access to all documents

Improve your grades

Join milions of students

By signing up you accept Terms of Service and Privacy Policy

Earthquakes and Tsunami Formation

GCSE Geography Hazardous Earth past papers often include questions about earthquake mechanics and tsunami formation.

Earthquake occurrence:

Pressure builds up along fault lines
When the pressure exceeds the friction holding the plates together, they suddenly shift
Energy is released in the form of seismic waves

Earthquake characteristics:

Magnitude: Measured on the Richter scale (logarithmic)
Depth: Shallow earthquakes (close to surface) are often more severe
Location: Varies based on plate boundary type

Vocabulary: The focus is the point within the Earth where an earthquake originates, while the epicenter is the point on the Earth's surface directly above the focus.

Tsunami formation process:

An earthquake occurs under the ocean, jolting the oceanic crust
The water above the plate is displaced
This displacement creates a series of waves that travel outward from the epicenter
In deep water, tsunamis travel fast but with low amplitude
As the waves approach shallower coastal areas, they slow down due to friction with the seabed
This slowing causes the waves to increase in height, forming a wall of water
Tsunami waves can reach heights of 10 to 100 feet when they make landfall

Highlight: Understanding tsunami formation is crucial for coastal communities in tectonically active regions to prepare for and mitigate potential impacts.

Sign up to see the content. It's free!

Access to all documents

Improve your grades

Join milions of students

By signing up you accept Terms of Service and Privacy Policy

Earthquake Impacts and Management Strategies

Japan Earthquake 2011 (Developed country):

Magnitude: 9.0
Focus depth: 30km
Epicenter: 70km from coast in Sendai Bay

Primary impacts:

15,900 deaths (93% from drowning)
2,800 missing
6,150 injured
350,000 homeless

Secondary impacts:

Two nuclear reactors went into meltdown
Airports closed
Motorways damaged
Oil refinery set on fire
$235 billion in damage (costliest earthquake in history)

Haiti Earthquake 2010 (Developing country):

Magnitude: 7.0
Focus depth: 13km
Epicenter: 25km from Port-au-Prince (population 2.5 million)

Primary impacts:

316,000 deaths
300,000 injured
1 million homeless

Secondary impacts:

Cholera outbreak
1/5 of jobs lost
Factories and businesses destroyed
Port, communication, and roads damaged and blocked

Highlight: The stark difference in death tolls despite the lower magnitude of the Haiti earthquake highlights the importance of infrastructure and preparedness in mitigating earthquake impacts.

Earthquake management strategies:

Short-term relief:

Providing emergency shelter (e.g., tents, temporary housing)
Distributing food, water, and medical supplies
Search and rescue operations

Long-term planning:

Training and funding emergency services
Implementing building codes for earthquake-resistant structures
Developing and maintaining early warning systems

Preparation:

Public education on earthquake safety
Regular earthquake drills
Creating and updating evacuation plans

Example: Japan's extensive earthquake preparation, including strict building codes and public education, helped limit the death toll despite the earthquake's massive magnitude.

Understanding these impacts and management strategies is crucial for answering Understanding tectonic hazards in geography Edexcel B questions and preparing for future seismic events.

Sign up to see the content. It's free!

Access to all documents

Improve your grades

Join milions of students

By signing up you accept Terms of Service and Privacy Policy

Page 8: Tropical Cyclone Formation

Details the process of tropical cyclone development.

Definition: The Coriolis effect causes tropical cyclones to spin clockwise in the Southern Hemisphere and counterclockwise in the Northern Hemisphere.

Highlight: Warm ocean temperatures of at least 26-27°C are required for tropical cyclone formation.

Sign up to see the content. It's free!

Access to all documents

Improve your grades

Join milions of students

By signing up you accept Terms of Service and Privacy Policy

Earth's Structure and Plate Tectonics

The Earth's structure consists of several layers, each with unique characteristics. Understanding tectonic hazards in geography Edexcel B requires knowledge of these layers and their properties.

Vocabulary: Lithosphere - The solid outer layer of the Earth, comprising the crust and uppermost mantle.

The layers of the Earth, from outermost to innermost, are:

Crust (0-100km thick)
Mantle (liquid/solid, 900-1600°C)
Outer core (liquid, 4000-5000°C)
Inner core (solid, 5400°C)

Convection currents in the mantle, generated by heat from radioactive decay in the core, drive plate tectonics. This process involves:

Heating of the fluid asthenosphere
Rising of less dense hot liquid
Cooling and sinking of denser material
Continuous cycle pushing and pulling plates

Highlight: Convection currents bbc Bitesize Geography explains this process in detail for students.

The three main types of plate boundaries are:

Divergent (plates move apart)
Convergent (plates collide)
Conservative (plates slide past each other)

Definition: Plate boundaries bbc Bitesize defines these as areas where tectonic plates meet and interact.

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Knowunity is the #1 education app in five European countries

Knowunity has been named a featured story on Apple and has regularly topped the app store charts in the education category in Germany, Italy, Poland, Switzerland, and the United Kingdom. Join Knowunity today and help millions of students around the world.

Download in

Google Play

Download in

App Store

4.9+

Average app rating

17 M

Pupils love Knowunity

#1

In education app charts in 17 countries

950 K+

Students have uploaded notes

Still not convinced? See what other students are saying...

iOS User

I love this app so much, I also use it daily. I recommend Knowunity to everyone!!! I went from a D to an A with it :D

Philip, iOS User

The app is very simple and well designed. So far I have always found everything I was looking for :D

Lena, iOS user